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Aerial photo of Salt River, Arizona with a meandering river surrounded by brown alluvium
Example of Alluvium
Example of Alluvium
Example of Alluvium

Alluvium visible in Salt River, Arizona (Photo by Sharon Reynolds, Arizona State University)

Alluvium visible in Salt River, Arizona (Photo by Sharon Reynolds, Arizona State University)

Drawing of Isaac Newton sitting on a hill under an apple tree
Newton Gravity
Newton Gravity
Newton Gravity

Illustration of Isaac Newton sitting under an apple tree, a reference to the well-known story of the epiphany Newton had when an apple fell on his head and lead to him discovering gravity.

Illustration of Isaac Newton sitting under an apple tree, a reference to the well-known story of the epiphany Newton had when an apple fell on his head and lead to him discovering gravity.

Photo of a snowy area with an instrument placed on the ground.  The instrument looks like a small pyramid on top of a tripod.
Geodesy
Geodesy
Geodesy

 

Geodesy is the science of determining the size and shape of the earth and the precise location of points on its surface.

 

Geodesy is the science of determining the size and shape of the earth and the precise location of points on its surface.

Blurry table of the geologic time scale
Geologic Time Scale
Geologic Time Scale
Geologic Time Scale

The geologic time scale showing each eon, era, period, epoch, and their associated ages.

The geologic time scale showing each eon, era, period, epoch, and their associated ages.

Photo of mountains in Zion Canyon with trees in the foreground
Photo of Zion Canyon (Geology)
Photo of Zion Canyon (Geology)
Photo of Zion Canyon (Geology)

Photo of Zion Canyon located in Zion National Park in Utah, United States. (Image courtesy of Justin Gould)

Photo of Zion Canyon located in Zion National Park in Utah, United States. (Image courtesy of Justin Gould)

Photo of mountains in the Grand Canyon
Photo of Grand Canyon (Geomorphology)
Photo of Grand Canyon (Geomorphology)
Photo of Grand Canyon (Geomorphology)

Photo of the Grand Canyon located in Grand Canyon National Park, Arizona, Untied States.

Photo of the Grand Canyon located in Grand Canyon National Park, Arizona, Untied States.

Photo of GPS site with a white instrument on a white tripod and a solar panel
GPS Site (Geophysics)
GPS Site (Geophysics)
GPS Site (Geophysics)

Photo of GPS site with instrument on a tripod and a solar panel. (Photo by John Galetzka, U.S. Geological Survey)

Photo of GPS site with instrument on a tripod and a solar panel. (Photo by John Galetzka, U.S. Geological Survey)

Photo of a bridge over a valley with a semi-transparent textbox labelled "www.worldweb.com. Photo c Jim Forrest"
Bridge (Geotechnical)
Bridge (Geotechnical)
Bridge (Geotechnical)

Photo of bridge.  Geotechnical means referring to the use of scientific methods and engineering principles to acquire, interpret, and apply knowledge of earth materials for solving engineering problems.  

Photo of bridge.  Geotechnical means referring to the use of scientific methods and engineering principles to acquire, interpret, and apply knowledge of earth materials for solving engineering problems.  

Crustal block diagram with the down-dropped blocks labelled as "graben" and the upthrown blocks labelled as "horst" between faults
Horst and Graben Diagram
Horst and Graben Diagram
Horst and Graben Diagram

Horst and graben diagram. A graben is a down-dropped block of the earth's crust resulting from extension, or pulling, of the crust. 

Horst and graben diagram. A graben is a down-dropped block of the earth's crust resulting from extension, or pulling, of the crust. 

Globe diagram with great circle around the globe with a dotted segment showing the shortest distance between two locations
Great Circle
Great Circle
Great Circle

Diagram of great circle. The shortest path between two points on the surface of a sphere lies along a great circle.

Diagram of great circle. The shortest path between two points on the surface of a sphere lies along a great circle.

Graph with scattered dots with a diagonal line going downward from left to right in between the dots
Least Squares Fit Plot
Least Squares Fit Plot
Least Squares Fit Plot

Plot showing least squares fit. When plotting data points on a graph, the least-squares-fit is the line or curve that comes closest to going through all the points.

Plot showing least squares fit. When plotting data points on a graph, the least-squares-fit is the line or curve that comes closest to going through all the points.

Block diagram showing the left coastal block moving forward and parallel as the right block moves away
Left-Lateral Motion Diagram
Left-Lateral Motion Diagram
Left-Lateral Motion Diagram

Diagram of left-lateral motion on fault. If you were to stand on the fault and look along its length, this is a type of strike-slip fault where the left block moves toward you and the right block moves away. See also right-lateral. 

Diagram of left-lateral motion on fault. If you were to stand on the fault and look along its length, this is a type of strike-slip fault where the left block moves toward you and the right block moves away. See also right-lateral. 

Photo of a leaning transmission tower being held up by lifeline cables in a wooded area
Leaning Transmission Tower with Lifelines
Leaning Transmission Tower with Lifelines
Leaning Transmission Tower with Lifelines

Photo of a leaning transmission tower being held up by lifelines. Lifelines are structures that are important or critical for a community to function, such as roadways, pipelines, powerlines, sewers, communications, and port facilities.

Photo of a leaning transmission tower being held up by lifelines. Lifelines are structures that are important or critical for a community to function, such as roadways, pipelines, powerlines, sewers, communications, and port facilities.

Photo of sand being ejected through cracks, forming holes along railroad tracks
Liquefaction Example
Liquefaction Example
Liquefaction Example

Sand ejected through a crack forming a series of sand boils along the railroad tracks adjacent to Deschutes Parkway in Olympia. 

Sand ejected through a crack forming a series of sand boils along the railroad tracks adjacent to Deschutes Parkway in Olympia. 

Cross-section of depths -16720 to -16780 with color-coded lithology sections and descriptions of each section
Lithology Cross-Section
Lithology Cross-Section
Lithology Cross-Section

Lithologic cross-section example with descriptions of lithology at different depths. 

Lithologic cross-section example with descriptions of lithology at different depths. 

Diagram of a locked fault (blue) going  at a labelled coastline with a curbed
Locked Fault
Locked Fault
Locked Fault

Diagram of a locked fault showing the shortening and uplift at a coastline. A locked fault is a fault that is not slipping because frictional resistance on the fault is greater than the shear stress across the fault (it is stuck).

Diagram of a locked fault showing the shortening and uplift at a coastline. A locked fault is a fault that is not slipping because frictional resistance on the fault is greater than the shear stress across the fault (it is stuck).

Diagram of a figure with a cube form made up of smaller cubes bent into waves and then going straight
Love Wave
Love Wave
Love Wave

A Love wave is a surface wave having a horizontal motion that is transverse (or perpendicular) to the direction the wave is traveling.

A Love wave is a surface wave having a horizontal motion that is transverse (or perpendicular) to the direction the wave is traveling.

Diagram of a mid-ocean ridge showing magnetic polarity progression
Magnetic Polarity
Magnetic Polarity
Magnetic Polarity

A magnetic polarity reversal is a change of the earth's magnetic field to the opposite polarity. This has occurred at irregular intervals during geologic time. Polarity reversals can be preserved in sequences of magnetized rocks and compared with standard polarity-change time scales to estimate geologic ages of the rocks.

A magnetic polarity reversal is a change of the earth's magnetic field to the opposite polarity. This has occurred at irregular intervals during geologic time. Polarity reversals can be preserved in sequences of magnetized rocks and compared with standard polarity-change time scales to estimate geologic ages of the rocks.

Magnitude plots with rainbow color gradients to compare the magnitude of two earthquakes
Magnitude Comparison
Magnitude Comparison
Magnitude Comparison

Compare the fault area of the magnitude 7.3 (top) with that of the magnitude 5.6 (smallest one near the bottom).

Compare the fault area of the magnitude 7.3 (top) with that of the magnitude 5.6 (smallest one near the bottom).

Two fault lines with circles showing their aftershocks
Landers Fault and Hector Mine Fault Aftershocks
Landers Fault and Hector Mine Fault Aftershocks
Landers Fault and Hector Mine Fault Aftershocks

The Landers fault (red lines at left) and the Hector Mine fault and its aftershocks (red lines and circles at right). The Hector Mine earthquake was a magnitude 7.1, and it produced thousands of aftershocks.

The Landers fault (red lines at left) and the Hector Mine fault and its aftershocks (red lines and circles at right). The Hector Mine earthquake was a magnitude 7.1, and it produced thousands of aftershocks.

Map of the San Francisco Bay Area, California with colored spots showing liquefaction potential
Liquefaction Potential Bay Area
Liquefaction Potential Bay Area
Liquefaction Potential Bay Area

Liquefaction potential map of the San Francisco Bay Area, California. (Image courtesy of the Association of Bay Area Governments-ABAG)

Liquefaction potential map of the San Francisco Bay Area, California. (Image courtesy of the Association of Bay Area Governments-ABAG)